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Modeling of bottom backscattering from three-dimensional volume inhomogeneities and comparisons with experimental data

机译:基于三维体积不均匀性的底部反向散射建模以及与实验数据的比较

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摘要

In this paper, backscattering from 3D volume inhomogeneities in the seabed is modeled and the results compared with experimental data at 250-650 Hz. The experiment was part of the Acoustic Reverberation Special Research Program (ARSRP) and the data were obtained in a sediment pond on the western flank of the Mid-Atlantic Ridge. A volume scattering model based on first-order perturbation theory is developed incorporating contributions from both sound speed and density fluctuations. With the propagators, i.e., the Green's functions, handled accurately through numerical wave number integration and random fluctuations generated effectively by a new scheme modified from the spectral method, the model is capable of simulating monostatic, backscattered fields in the frequency domain as well as in the time domain owing to 3D volumetric sediment inhomogeneities. The model compares favorably and consistently with the ARSRP backscattering data over the entire frequency band, with the fluctuations of sound speed and density in two irregular sediment layers, identified from the data analysis, described by a power-law type of power spectrum.
机译:在本文中,对海床中3D体积不均匀性造成的反向散射进行了建模,并将结果与​​250-650 Hz的实验数据进行了比较。该实验是声学混响特别研究计划(ARSRP)的一部分,数据是从大西洋中脊西翼的沉积池中获得的。建立了基于一阶微扰理论的体积散射模型,该模型结合了声速和密度波动的贡献。借助传播器(即格林函数),通过数值波数积分和通过对频谱方法进行修改的新方案有效产生的随机波动,可以准确地处理该模型,该模型能够在频域以及时域是由于3D体积沉积物的不均匀性。该模型与整个频带上的ARSRP背向散射数据进行了良好且一致的比较,并通过数据定律(由功率定律类型的功率谱描述)确定了两个不规则沉积物层中声速和密度的波动。

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